基于反升降的陆地 relief 演化分析
地球物理
2025-07-08 v1
摘要
通过考察地震能量理论和火山能量理论，我们理解到内部能量与外部能量在有利地形条件下的相互作用导致了数以百万计的变形在地质时间尺度上持续发生。因此，本研究旨在基于 Claudio Valverde Ramirez 提出的理论来理解地球表面的演化。本研究引入了反升降概念，这一概念解释了山脉的形成、陆地 relief 的持续和不规则动力学，以及大陆和岛屿海岸线的持续重塑，这些过程也取决于水体的流动性。
引用
@article{arxiv.2507.03173,
title = {Analysis of the evolution of terrestrial relief through inverse elevation transition},
author = {Yulisa Valverde and Milton Valverde and Jhair Tarazona and Giorgio Tarazona and Yehosua Tarazona},
journal= {arXiv preprint arXiv:2507.03173},
year = {2025}
}
备注
This paper introduces the Inverse Elevation Transition (TIC), a geodynamic model based on TES and TEV theories. It proposes that Earth's relief evolves through internal energy-driven geological combustion. The study outlines mountain formation in stages and explains surface changes, aseismic zones, and sea level shifts over geological time